ScienceDaily
February 7, 2012
The MARSIS radar was deployed in 2005 and has been collecting data ever since. Jérémie Mouginot, Institut de Planétologie et d'Astrophysique de Grenoble (IPAG) and the University of California, Irvine, and colleagues have analysed more than two years of data and found that the northern plains are covered in low-density material.
(Image above): New results from the MARSIS radar on Mars Express give strong evidence for a former ocean of Mars. The radar detected sediments reminiscent of an ocean floor inside previously identified, ancient shorelines on the red planet. The ocean would have covered the northern plains billions of years ago. Credits: ESA, C. Carreau
Two oceans have been proposed: 4 billion years ago, when warmer conditions prevailed, and also 3 billion years ago when subsurface ice melted, possibly as a result of enhanced geothermal activity, creating outflow channels that drained the water into areas of low elevation.
"MARSIS penetrates deep into the ground, revealing the first 60-80 metres of the planet's subsurface," says Wlodek Kofman, leader of the radar team at IPAG.
"Throughout all of this depth, we see the evidence for sedimentary material and ice."
The sediments revealed by MARSIS are areas of low radar reflectivity. Such sediments are typically low-density granular materials that have been eroded away by water and carried to their final destination.
This later ocean would however have been temporary. Within a million years or less, Dr Mouginot estimates, the water would have either frozen back in place and been preserved underground again, or turned into vapour and lifted gradually into the atmosphere.
"I don't think it could have stayed as an ocean long enough for life to form."
In order to find evidence of life, astrobiologists will have to look even further back in Mars' history when liquid water existed for much longer periods.
"This adds new pieces of information to the puzzle but the question remains: where did all the water go?"
Mars Express continues its investigation.
Story Source:
The above story is reprinted from materials provided by European Space Agency.
Journal Reference:
Jérémie Mouginot, Antoine Pommerol, Pierre Beck, Wlodek Kofman, Stephen M. Clifford. Dielectric map of the Martian northern hemisphere and the nature of plain filling materials. Geophysical Research Letters, 2012; 39 (2) DOI: 10.1029/2011GL050286
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